Taylor Peak (Grand County, Colorado)

Taylor Peak

13,153 ft. Taylor Peak, 12,486 ft. Otis Peak, 12,713 ft. Hallet Peak and 12,324 ft. Flat Top Mountain after an early Fall snow storm, within Rocky Mountain National Park, Colorado. | Robert Waltman

Taylor Peak is a 13,156-foot (4,010-meter) summit on the Continental Divide in Rocky Mountain National Park, Colorado. Rising at the head of dramatic Loch Vale between Powell Peak and Hallett Peak, the mountain combines broad alpine tundra on its western slopes with a much steeper eastern face overlooking glaciers, lakes, and some of the most rugged terrain in the Front Range.

The Grand County designation helps distinguish this Taylor Peak from another Colorado summit of the same name in the Elk Mountains. This Taylor Peak actually sits along the Grand–Larimer county boundary, with the Continental Divide forming the dividing line. Its summit is accessible by a challenging Class 2 route through Glacier Gorge and Andrews Glacier, while steeper snow-and-ice routes such as Taylor Glacier provide significantly more technical alternatives.

πŸ”οΈ Overview

Taylor Peak occupies a spectacular position in the central portion of Rocky Mountain National Park. The mountain rises along the Continental Divide, with gentler tundra terrain falling west toward Grand County and dramatic cliffs and glacial cirques dropping east toward Loch Vale in Larimer County.

At 13,156 feet, Taylor Peak is one of the park’s twenty named summits above 13,000 feet. It is lower than nearby Powell Peak, McHenrys Peak, Chiefs Head Peak, and Longs Peak, but still stands among the highest mountains in the Front Range.

Modern LiDAR has refined the summit elevation to approximately 13,156.3 feet. Its prominence is about 416 feet, while its isolation is just over one mile. Powell Peak, immediately southeast, is the nearest higher neighbor.

Taylor Peak is particularly appealing to experienced hikers because it receives far less traffic than many famous Rocky Mountain National Park destinations. There is no maintained trail to the summit itself, and reaching the top requires a long wilderness approach, snow travel during much of the year, and off-trail navigation above Andrews Pass.

⚑ Fast Facts

FactDetails
ContinentNorth America
CountryUnited States
State/ProvinceColorado
County/RegionGrand and Larimer counties
Protected AreaRocky Mountain National Park
Wilderness AreaRocky Mountain National Park Wilderness
Mountain RangeFront Range, Rocky Mountains
ParentsFront Range, Rocky Mountains
Elevation13,156 ft / 4,010 m
LiDAR Elevation13,156.3 ft / 4,010.0 m
Prominence416 ft / 127 m
Isolation1.02 mi / 1.64 km
Nearest Higher Neighbor (NHN)Powell Peak
Key ColApprox. 12,740 ft / 3,883 m
Coordinates40.27471Β° N, 105.68033Β° W
USGS QuadrangleMcHenrys Peak
Major DivideContinental Divide
Nearby PeakHallett Peak
Primary Standard RouteAndrews Glacier / Andrews Pass
Standard Route DifficultyClass 2
Typical Round TripApprox. 12.4 mi / 20 km
Typical Elevation GainApprox. 4,000–4,200 ft / 1,220–1,280 m
Historic NameThe Bangs
Fun FactWater falling on opposite sides of Taylor Peak eventually drains toward different oceans.

πŸ“ Location

Taylor Peak lies near the center of Rocky Mountain National Park, southwest of Estes Park and east of Grand Lake.

The summit stands directly on the Continental Divide, which also forms the boundary between Grand County on the west and Larimer County on the east in this area.

This geographic position explains why some databases identify Taylor Peak primarily with Grand County while others list both counties.

The mountain rises at the head of Loch Vale, a spectacular glacial basin accessed from the Glacier Gorge trail system. Its eastern slopes form part of the enormous wall surrounding The Loch, while the western side descends much more gently across high tundra.

Powell Peak lies directly southeast along the Continental Divide. Hallett Peak and Otis Peak rise to the north, while McHenrys Peak, Chiefs Head Peak, Pagoda Mountain, and Longs Peak dominate the skyline farther south.

πŸ“ Elevation & Prominence

Taylor Peak reaches 13,156.3 feet (4,010 meters) according to LiDAR-refined elevation data.

Older topographic sources frequently list the mountain at 13,153 or 13,158 feet, explaining the different figures that may still appear in guidebooks and older online references.

The summit has approximately 416 feet (127 meters) of topographic prominence.

Its key saddle lies at about 12,740 feet (3,883 meters) along the ridge connecting Taylor Peak with higher terrain.

Topographic isolation is approximately 1.02 miles (1.64 kilometers).

The nearest higher neighbor is Powell Peak, which reaches approximately 13,208 feet and stands southeast along the Continental Divide.

Taylor Peak therefore qualifies as a distinct named summit but is closely integrated into the much larger chain of high peaks forming the backbone of Rocky Mountain National Park.

🌎 The Continental Divide

Taylor Peak occupies one of the most important geographic boundaries in North America: the Continental Divide.

The divide runs for approximately 42 miles through Rocky Mountain National Park, separating watersheds that eventually reach different oceans.

Water draining west from Taylor Peak ultimately enters tributaries of the Colorado River, which flows southwest toward the Gulf of California and the Pacific Ocean drainage system.

Water draining east enters streams flowing toward the South Platte River, which eventually reaches the Missouri and Mississippi rivers before emptying into the Gulf of Mexico and Atlantic drainage system.

Standing on Taylor Peak therefore places a hiker directly on the hydrological backbone of the continent.

The Continental Divide also explains the mountain’s contrasting terrain. Glacial erosion has carved deep basins on the eastern side, while the western slopes retain broader expanses of alpine tundra.

πŸͺ¨ Geology

Taylor Peak is built from the ancient crystalline rocks characteristic of much of Rocky Mountain National Park.

The oldest rocks in the park are approximately 1.7 to 1.8 billion years old. Ancient sediments were buried, compressed, heated, and transformed into metamorphic rocks such as gneiss and schist.

Large bodies of magma later intruded into these older rocks. As the magma cooled underground roughly 1.4 billion years ago, it crystallized into granitic rock.

These ancient rocks form much of the foundation of today’s Front Range.

The modern mountains are far younger than the rock itself. Major uplift during the formation of the Rocky Mountains raised the region, while millions of years of erosion gradually exposed the ancient crystalline core.

Taylor Peak therefore presents a striking geological contrast: the mountain landscape itself is geologically young compared with the nearly two-billion-year-old rocks from which it is built.

🧊 Glacial Sculpting

Glaciers played an enormous role in shaping Taylor Peak and the surrounding Loch Vale landscape.

During repeated Ice Age glaciations, large masses of ice flowed through the high valleys of what is now Rocky Mountain National Park.

Moving glaciers carried rocks, sand, and other debris that acted like enormous sheets of sandpaper, grinding into the underlying bedrock.

The result can be seen throughout the Taylor Peak area.

Cirques were carved beneath steep mountain walls, valleys developed characteristic U-shaped profiles, and moraines accumulated where glaciers deposited transported debris.

Several small glaciers and permanent or semi-permanent ice features remain in Rocky Mountain National Park today, preserving a much smaller version of the processes that once transformed the entire region.

Taylor Peak is especially associated with Andrews Glacier and Taylor Glacier, two dramatically different routes into its upper mountain terrain.

🧊 Andrews Glacier

Andrews Glacier lies north of Taylor Peak between Taylor and Otis Peak and provides the most commonly used high route to the summit.

Hikers approach through Glacier Gorge, passing The Loch before climbing toward Andrews Tarn and Andrews Glacier.

The glacier occupies a steep but relatively broad chute leading to Andrews Pass on the Continental Divide.

Depending on the season, the route may involve travel over firm snow, soft snow, ice, or increasingly exposed rock and debris.

Once Andrews Pass is reached, the technical character eases considerably. Climbers turn south and follow the broad western side of Taylor Peak over tundra and boulder-strewn terrain toward the summit.

This route demonstrates the mountain’s dramatic asymmetry: the western side is relatively gentle while the cliffs immediately east plunge into Loch Vale.

πŸ₯Ύ Taylor Peak via Andrews Glacier

The standard Taylor Peak route usually begins at the Glacier Gorge Trailhead along Bear Lake Road.

The Colorado Mountain Club describes the route as approximately 12.4 miles round trip with nearly 4,200 feet of elevation gain.

Another detailed route guide calculates roughly 3,975 feet of gain, with differences depending on exact route choice and measurement method.

From Glacier Gorge, hikers follow established trails toward The Loch, one of the most beautiful high lakes in Rocky Mountain National Park.

The route then branches toward Andrews Creek and climbs increasingly rugged terrain toward Andrews Tarn and Andrews Glacier.

After ascending the glacier or adjacent terrain to Andrews Pass, hikers reach the Continental Divide.

The final ascent turns south across approximately a mile of tundra and rock toward Taylor Peak.

The standard route is generally considered Class 2, but snow conditions can add mountaineering difficulty well beyond ordinary hiking.

πŸ§— Taylor Glacier

Taylor Glacier provides a dramatically more serious route on the mountain’s eastern side.

The glacier rises directly beneath Taylor Peak at the head of Loch Vale and forms a steep snow-and-ice couloir.

Traditional Colorado mountaineering descriptions rate the route around Class 3 with steep snow and ice.

The climb gains roughly 1,200 vertical feet and becomes progressively steeper, reportedly approaching approximately 60 degrees near the top under some conditions.

Cornices can form near the upper edge, creating an additional obstacle and substantial objective hazard.

Taylor Glacier should therefore not be confused with the easier Andrews Glacier approach.

It is an alpine snow-and-ice climb requiring appropriate conditions, equipment, experience, route assessment, and the ability to respond to changing hazards.

The mountain’s technical character was illustrated again in 2023 when Rocky Mountain National Park rangers conducted a helicopter rescue after a climber was injured in a roped fall on a mixed route on Taylor Peak.

πŸ₯Ύ Loch Vale Approach

Most Taylor Peak climbs from the east begin through Glacier Gorge.

The trail climbs past Alberta Falls and continues toward the junction leading to Mills Lake and The Loch.

The Loch lies beneath an extraordinary amphitheater of mountains and rock formations.

Taylor Peak forms part of the high western wall, while Otis Peak, Thatchtop Mountain, The Sharkstooth, Powell Peak, McHenrys Peak, and other summits surround the greater Glacier Gorge area.

The maintained trail system ends long before Taylor Peak’s summit.

Beyond the established routes near Andrews Creek, hikers enter increasingly rugged alpine terrain where route-finding and mountain judgment become important.

This transition from popular hiking trail to remote mountaineering terrain is part of what makes Taylor Peak such an interesting objective.

🌿 Flora & Fauna

Taylor Peak rises entirely into the alpine tundra zone on its upper slopes.

In Rocky Mountain National Park, treeline generally occurs between about 11,000 and 11,500 feet, depending on exposure and local conditions.

Above that elevation, strong winds, low temperatures, short summers, and thin soils prevent trees from growing.

Alpine plants survive by remaining close to the ground. Cushion plants and other compact species avoid some of the strongest wind, while deep roots help anchor vegetation in rocky soil.

Wildflowers found in the park’s alpine tundra include alpine avens, alpine forget-me-not, alpine phlox, moss campion, sky pilot, alpine paintbrush, and alpine sunflower.

Vegetation is extremely fragile. Plants may take decades to recover from trampling, so hikers should use durable rock surfaces whenever practical during off-trail travel.

🐏 Wildlife

The alpine environment surrounding Taylor Peak supports a surprising variety of wildlife.

American pikas inhabit talus slopes throughout Rocky Mountain National Park and are well adapted to cold alpine conditions. They remain active during winter rather than hibernating and collect plants during summer to form stored hay piles.

Yellow-bellied marmots are also characteristic residents of rocky alpine terrain.

Bighorn sheep may travel through high mountain areas, while elk often climb into alpine tundra during summer to feed and escape warmer temperatures.

Birds of the high country include white-tailed ptarmigan, brown-capped rosy-finches, horned larks, water pipits, ravens, and other species adapted to the exposed alpine environment.

Wildlife should be observed from a distance, and feeding animals is prohibited within Rocky Mountain National Park.

πŸŒ„ Summit Views

Taylor Peak offers exceptional views despite receiving much less attention than many neighboring mountains.

Looking south along the Continental Divide, Powell Peak dominates the immediate skyline.

Beyond it rise McHenrys Peak, Pagoda Mountain, Chiefs Head Peak, and Longs Peak.

To the north are Otis Peak and Hallett Peak.

The eastern view is especially dramatic. Loch Vale lies far below, surrounded by steep rock walls and sharp formations including The Sharkstooth and Thatchtop Mountain.

To the west, the terrain changes character completely. Broad tundra slopes descend toward the Colorado River side of Rocky Mountain National Park, with distant ranges visible beyond the Continental Divide under clear conditions.

The summit therefore provides an outstanding perspective on the contrasting eastern and western sides of the Front Range.

🌀️ Best Time to Climb

For hikers seeking the simplest snow-free conditions, mid-summer through early fall is generally the most practical period for Taylor Peak.

July, August, and early September usually provide the greatest opportunity for exposed tundra and rock on the upper mountain, although snowfields can persist throughout summer.

The Andrews Glacier route may be more straightforward as a snow climb earlier in the season when consolidated snow provides a continuous surface.

Conditions vary substantially from year to year.

Winter and spring ascents require additional skills and equipment, including an understanding of avalanche conditions and winter navigation.

Regardless of season, Taylor Peak should be approached as an alpine mountain rather than an ordinary hiking destination.

β›ˆοΈ Thunderstorms & Weather

Summer thunderstorms are among the most important hazards on Taylor Peak.

The summit and surrounding Continental Divide provide virtually no shelter from lightning.

Storms commonly develop during summer afternoons, making early starts essential for long alpine objectives.

A hiker starting from Glacier Gorge still has many miles and several thousand feet of climbing before reaching the summit, so timing must account for the lengthy approach.

Clouds can also obscure the Continental Divide rapidly, complicating navigation.

Snow, hail, high wind, and freezing temperatures are possible even during summer.

Visitors should check the current mountain forecast before departure and be willing to turn around if conditions begin deteriorating.

🫁 Altitude

Taylor Peak exceeds 13,000 feet, high enough for altitude to noticeably affect many hikers.

Visitors arriving directly from lower elevations may experience headache, fatigue, nausea, reduced appetite, dizziness, or unusually slow hiking speed.

Acclimatization is particularly valuable because the standard route is long and already requires roughly 4,000 feet of climbing.

Hydration, adequate food, conservative pacing, and time spent at moderate altitude beforehand can help.

Serious or worsening altitude symptoms are a reason to descend rather than continue upward.

Even experienced hikers may find the final tundra climb much slower than expected because of the thin air.

⚠️ Safety

Taylor Peak should be considered a serious backcountry mountain objective.

The standard Andrews Glacier route involves a long approach, off-trail travel, high altitude, snow or ice during much of the year, and exposure to rapidly changing weather.

Depending on conditions, hikers may need traction, an ice axe, helmet, or other mountaineering equipment. Anyone traveling on steep snow should know how to use that equipment rather than simply carrying it.

Taylor Glacier is substantially more technical and should only be attempted by experienced alpine climbers.

Rockfall can occur on steep terrain, particularly as seasonal snow melts.

Navigation is another concern. Clouds and thunderstorms can obscure landmarks quickly along the broad Continental Divide.

Because the route travels through designated wilderness far from roads, rescue may require considerable time and resources.

🎫 Permits & Park Regulations

A special climbing permit is not normally required for a day ascent of Taylor Peak, but visitors must comply with Rocky Mountain National Park entrance and access requirements.

Because the standard Andrews Glacier route begins along Bear Lake Road, summer visitors may need a seasonal Timed Entry + Bear Lake Road reservation.

For the 2026 season, that reservation is required to enter the Bear Lake Road corridor between 5 a.m. and 6 p.m. from May 22 through October 18.

A standard park entrance pass or fee is also required.

Visitors beginning before the timed-entry window should verify the current rules before relying on early entry, as regulations can change from year to year.

Overnight wilderness trips require a wilderness camping permit.

Dogs are not permitted on Rocky Mountain National Park trails.

🚌 Getting There

The most common starting point is the Glacier Gorge Trailhead on Bear Lake Road.

Parking at Glacier Gorge is extremely limited and commonly fills very early.

Rocky Mountain National Park operates a seasonal shuttle system along Bear Lake Road. In 2026, the Bear Lake shuttle serves the Glacier Gorge Trailhead between late May and mid-October.

The Park & Ride lot can therefore be a practical alternative to attempting to park directly at the trailhead.

Taylor Peak climbers usually require an early start because the route is long and afternoon thunderstorms are common.

The Glacier Gorge Trailhead begins at approximately 9,185 feet, leaving nearly 4,000 feet of total climbing before reaching the summit.

🧭 Nearby Mountains & Attractions

Powell Peak rises immediately southeast of Taylor Peak and reaches approximately 13,208 feet. It is Taylor Peak’s nearest higher neighbor and is sometimes combined with Taylor in a longer summit day.

Hallett Peak rises north of Taylor Peak and forms one of Rocky Mountain National Park’s most recognizable mountain profiles above Bear Lake.

Otis Peak stands between Hallett Peak and Taylor Peak and overlooks Andrews Glacier.

McHenrys Peak rises farther south and reaches approximately 13,327 feet.

Longs Peak dominates the skyline farther southeast at 14,259 feet and is the highest mountain in Rocky Mountain National Park.

The Sharkstooth is a spectacular rock spire below Taylor Peak and one of the park’s classic technical climbing destinations.

The Loch provides a much easier hiking destination beneath Taylor Peak and offers dramatic views toward the surrounding Glacier Gorge mountains.

πŸ’‘ Fun Facts

Taylor Peak reaches 13,156 feet, placing it among Rocky Mountain National Park’s twenty named summits above 13,000 feet.

Modern LiDAR increased the commonly listed summit elevation by several feet compared with older topographic maps.

The peak sits directly on the Continental Divide and the boundary between Grand and Larimer counties.

Water on Taylor Peak’s western side ultimately drains toward the Colorado River, while water on the eastern side enters the Mississippi River drainage system.

The nearest higher neighbor is Powell Peak, only about one mile away.

Taylor Peak was historically known as The Bangs before its modern name became established.

Its western slopes consist largely of broad alpine tundra, while the eastern side drops dramatically into Loch Vale.

The easiest commonly used route reaches the summit through Andrews Glacier and Andrews Pass.

The much steeper Taylor Glacier provides a classic alpine snow-and-ice route below the summit.

Rocky Mountain National Park contains approximately 89,000 acres of alpine tundra, and Taylor Peak rises well within this harsh high-elevation ecosystem.

❓ Frequently Asked Questions

How high is Taylor Peak?

Modern LiDAR places Taylor Peak at approximately 13,156 feet (4,010 meters) above sea level.

Where is Taylor Peak?

Taylor Peak lies in Rocky Mountain National Park in Colorado, on the Continental Divide between Grand and Larimer counties.

Why is it called Taylor Peak (Grand County)?

Colorado has more than one mountain named Taylor Peak. The Grand County designation distinguishes this Front Range summit from another Taylor Peak farther southwest in the Elk Mountains.

What mountain range is Taylor Peak in?

Taylor Peak belongs to the Front Range of the Rocky Mountains.

What is the prominence of Taylor Peak?

Its topographic prominence is approximately 416 feet (127 meters).

What is the isolation of Taylor Peak?

Taylor Peak has approximately 1.02 miles (1.64 kilometers) of topographic isolation.

What is the nearest higher neighbor?

Powell Peak, immediately southeast, is the nearest higher neighbor.

Is Taylor Peak on the Continental Divide?

Yes. The summit lies directly on the Continental Divide.

Is Taylor Peak in Grand County or Larimer County?

The mountain sits along the Grand–Larimer county boundary. The Continental Divide forms the county line in this area.

How difficult is Taylor Peak?

The standard Andrews Glacier route is generally considered Class 2, but snow travel, route-finding, altitude, distance, and weather make it a serious alpine outing.

How long is the standard hike?

The Andrews Glacier route is approximately 12.4 miles round trip with roughly 4,000 to 4,200 feet of elevation gain.

Where does the Taylor Peak hike begin?

The standard route begins at the Glacier Gorge Trailhead along Bear Lake Road in Rocky Mountain National Park.

What is Taylor Glacier?

Taylor Glacier is a steep snow-and-ice route on Taylor Peak’s eastern side. It is considerably more technical than the standard Andrews Glacier approach.

Can you hike Taylor Peak without crossing snow?

Late summer may provide relatively snow-free conditions on much of the route, but snowfields can persist at high elevations. Conditions should always be checked before departure.

When is the best time to climb Taylor Peak?

Summer through early fall generally provides the easiest hiking conditions. Spring and early summer may offer good snow climbing but require additional mountaineering skills and equipment.

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